Continental Collision

Continental Collision is a tectonic plate interaction process in which two plates bearing buoyant continental lithosphere converge after the closure of an intervening ocean basin, terminating oceanic subduction and producing large-scale crustal thickening, deformation, and orogenesis.

2.1K

Publications

202.2K

Citations

5K

Authors

1.2K

Institutions

Publications per year

2017–2026

413

Authors

5K

  1. TG
    Taras Gerya

    ETH Zurich, Switzerland

    24 publications · 2.5K citations

    22

    h-index

  2. YZ
    Yong‐Fei Zheng

    University of Science and Technology of China, China

    25 publications · 2.7K citations

    22

    h-index

  3. PA
    Peter A. Cawood

    Monash University, Australia

    24 publications · 3.3K citations

    20

    h-index

  4. YN
    Yaoling Niu

    Durham University, United Kingdom

    18 publications · 3.7K citations

    17

    h-index

  5. MS
    M. Santosh

    China University of Geosciences (Beijing), China

    20 publications · 1.5K citations

    16

    h-index

1–5 of 5K

Venues

  1. Tectonics

    174 publications · 20.3K citations

    74

    h-index

  2. Geological Society London Special Publications

    147 publications · 15.8K citations

    68

    h-index

  3. Geology

    94 publications · 13.3K citations

    56

    h-index

  4. Tectonophysics

    121 publications · 9.4K citations

    56

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 64 publications · 11.9K citations

    51

    h-index

1–5